Journal
JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
Volume 117, Issue -, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2011JC007599
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Funding
- Oceanographic Section of the National Science Foundation
- National Science Foundation [IOS-0743903]
- National Oceanic Association Administration
- Division Of Ocean Sciences
- Directorate For Geosciences [752972] Funding Source: National Science Foundation
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Fish have been shown to produce high (10 to 48 mol %) magnesium calcite as part of the physiological mechanisms responsible for maintaining salt and water balance. The importance of this source to the marine carbon cycle is only now being considered. In this paper, we report the first measurements of the solubility of this CaCO3 in seawater. The resulting solubility (pK(sp)* = 5.89 +/- 0.09) is approximately two times higher than aragonite and similar to the high magnesium calcite generated on the Bahamas Banks (pK(sp)* = 5.90). This high solubility of fish-produced CaCO3 is a result of the high magnesium content and not a product of micro-environments created by microbial activity. This material is soluble in near surface waters, contributing to the input of carbonate to surface ocean waters, and may at least partially explain the observed increase in total alkalinity above the aragonite saturation horizon.
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